Moon’s Magnetosphere: ???

IMO as the earth and moon moved closer together the core of the moon shifted and a tidal lock was established. The forces increased until the cor material was coming out in the form of massive eruptions. That was the core and the material continued until the earth was it's destination. The GOM and Hudson Bay were where the biggest 'blobs' landed. Going to the core also expanded, the fragile crust cracked along the same lines we find in the 40,000 miles of Oceanic Rifts that are still spreading.
Once the moon was 'lighter' the speed was enough to allow the moon to start moving away, like it is still doing today.

[link to sputniknews.com (secure)]
Warning of Things to Come? Moon’s Magnetosphere, Once Twice as Strong as Earth’s, Died Mysteriously
The magnetosphere is the main force protecting Earth from the powerful solar radiation which constantly bombards our planet. Without it, our planet would quickly become an uninhabitable wasteland.

Researchers at the Massachusetts Institute of Technology have discovered that the Moon once had a powerful magnetic field twice as strong as that of Earth, but that it was weakened before petering out completely about one billion years ago.

According to the researchers, who published their findings in this month’s issue of the Science Advances journal, the Moon’s magnetic field was powered by a powerful dynamo effect generated by a phenomenon known as ‘core crystallization.’ This phenomenon is said to have worked as follows: as the moon’s inner core cooled and was crystalized, the core’s electronically charged fluid was stirred buoyantly, producing the dynamo effect.

Dr. Benjamin Weiss, MIT professor of Earth, Atmospheric and Planetary Sciences and the study’s coauthor, explained that the magnetic field “is this nebulous thing that pervades space, like an invisible field. We’ve shown that the dynamo that produced the Moon’s magnetic field died somewhere between 1.5 and 1 billion years ago, and seems to have been powered in an Earth-like way.”

Dr. Weiss and his colleagues were able to come up with an estimate regarding the former power of the Moon’s magnetic field using lunar rocks collected by NASA’s Apollo project, which showed that samples up to 4 billion years old gleamed with evidence of a strong magnetic field of roughly 100 microteslas (a unit of magnetic flux density). By comparison, Earth’s magnetic field is estimated at just half that – about 50 microteslas.

Later, the scientists studied other, ‘younger’ moon r

Last Edited by Wayfaring Stranger on 01/06/2020 03:51 PM